Open AccessSeasonal and solar cycle variations of the ionospheric peak electron density: Comparison of measurement and models
Author(s) -
Richards P. G.
Publication year - 2001
Publication title -
journal of geophysical research: space physics
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.67
H-Index - 298
eISSN - 2156-2202
pISSN - 0148-0227
DOI - 10.1029/2000ja000365
Subject(s) - equinox , solstice , ionosphere , southern hemisphere , middle latitudes , atmospheric sciences , solar maximum , northern hemisphere , noon , solar cycle , f region , variation (astronomy) , solar minimum , seasonality , environmental science , climatology , latitude , geology , physics , geodesy , plasma , astrophysics , solar wind , mathematics , geophysics , quantum mechanics , statistics
This paper examines the ability of empirical and physical models to reproduce the peak electron density of the midlatitude ionospheric F 2 region ( N m F 2 ) from 1976 to 1980. The data from all midlatitude stations show a tendency toward a semiannual variation in noon N m F 2 with peaks at the equinoxes for all levels of solar activity. The Southern Hemisphere semiannual variation is more pronounced than in the Northern Hemisphere primarily because the winter density is relatively low in the Southern Hemisphere. At most locations the equinox density peaks are approximately equal. However, the September peak is much weaker than the March peak at most Australian stations. This leads to a distinct longitudinal variation between the Australian and South American sectors. On the other hand, there is remarkably little longitudinal variation in the Northern Hemisphere. We present calculations from the field line interhemispheric plasma (FLIP) model from 1976 to 1980 at six representative midlatitude stations around the globe. The FLIP model reproduces the average seasonal and solar cyclical behavior of the measured N m F 2 remarkably well most of the time. The greatest differences of 50% occur at the March equinox in the South American region and at the September equinox in the Australian region during September solstice solar maximum. The international reference ionosphere (IRI) model reproduces the average N m F 2 even better than the FLIP model but, unlike the FLIP model, it has little day‐to‐day variation. A factor of 2 increase in the solar EUV ion production rate and in the atomic to molecular density ratio at the F 2 region peak height ( h m F 2 ) produces a factor of 4 increase in N m F 2 over a solar cycle. Most of this increase takes place before the average solar activity index ( F 10.7 ) reaches 175. At solar maximum in 1979 and 1980, there is little relationship between daily F 10.7 and N m F 2 . Changes in the atomic to molecular density ratio at h m F 2 are primarily responsible for the semiannual variation in the FLIP model N m F 2 . The inclusion of vibrationally excited N 2 in the FLIP model improves the relative seasonal and solar cycle N m F 2 variations in the FLIP model, but it causes the overall N m F 2 to be too low at most stations.